Chalcocite (Cu2S) is one of the most important copper sulfides and a classic collector species despite its softness and tendency to tarnish. -> ãã£ã«ã³ãµã€ãïŒCu2SïŒã¯ãæããããšå€è²ããããæ§è³ªã«ãããããããæãéèŠãªé ç¡«åç©ã®äžã€ã§ãããå€å žçãªã³ã¬ã¯ã¿ãŒçš®ã§ãã
Crystals are typically dark steelâgray to black with a bright metallic luster and often display spectacular pseudohexagonal forms caused by twinning. -> çµæ¶ã¯éåžžãæ¿ãéŒéç°è²ããé»è²ã§ãæããéå±å æ²¢ãæã¡ãåæ¶ã«ãã£ãŠçãã壮芳ãªåœå è§åœ¢ã®åœ¢ããã°ãã°ç€ºããŸãã
The best specimens show sharp, thick plates or rosettes (âwheelsâ), sometimes stacked or cyclically twinned into dramatic clusters. -> æè¯ã®æšæ¬ã¯ãéãåãæ¿ç¶ãŸãã¯ããŒãŒããç¶ïŒè»èŒªç¶ïŒã瀺ããæã«ã¯ç©ã¿éãããããã埪ç°çã«åæ¶åããŠãã©ãããã¯ãªç°ã圢æããŸãã
Most chalcocite in nature is massive or vein-filling ore, so fine, well-formed crystals are quite rare. -> èªç¶çã®ã»ãšãã©ã®ãã£ã«ã³ãµã€ãã¯å¡ç¶ãŸãã¯èç¶ã®é±ç³ã§ããããã现ãããããæŽã£ãçµæ¶ã¯ããªãçšã§ãã
When they do occurâespecially on contrasting light matrix like calcite or dolomiteâthey are striking, minimalist sculptures that anchor sulfide suites. -> ããããçŸãããšãã«ã¯ãç¹ã« calciteïŒæ¹è§£ç³ïŒã dolomiteïŒãããã€ãïŒã®ãããªæãããããªãã¯ã¹ãšå¯Ÿç §çãªå Žåã«ãç¡«åç©çŸ€ãæ¯ããå°è±¡çã§ããããªã¹ããªåœ«å»ã®ãããªæšæ¬ã«ãªããŸãã
Collectors prize chalcocite for these textbook twinned habits, brilliant luster, historic provenance, and the subtle peacock iridescence that can develop on old surfaces. -> ã³ã¬ã¯ã¿ãŒã¯ããããã®æç§æžçãªåæ¶ç¿æ§ãèŒãå æ²¢ãæŽå²çç±æ¥ãããã³å€ã衚é¢ã«çºçãã埮åŠãªåéå æ²¢ã®ããã«ãã£ã«ã³ãµã€ããé«ãè©äŸ¡ããŸãã
While chalcocite is a major ore of copper worldwide, crystal-quality material has been produced at only a handful of localities. -> ãã£ã«ã³ãµã€ãã¯äžççã«é ã®äž»èŠé±ç³ã§ãããçµæ¶åè³ªã®æšæ¬ã¯ããéãããç£å°ã§ã®ã¿çç£ãããŠããŸãã
The classic 19th-century finds from Cornwall (England) and Bristol, Connecticut set an early standardâmuseum-grade plates and rosettes that remain highly sought today. -> 19äžçŽã®ã³ãŒã³ãŠã©ãŒã«ïŒ EnglandïŒãšããªã¹ãã«ïŒã³ããã«ããå·ïŒã®å€å žçãªçºèŠã¯åæã®æšæºãæã¡ç«ãŠãŸããââãã¥ãŒãžã¢ã ã°ã¬ãŒãã®æ¿ç¶ããã³ããŒãŒããã¯ã仿¥ã§ãé«ãè©äŸ¡ãããŠããŸãã
In the late 20th century, Kazakhstanâs Dzhezkazgan mining district rejuvenated excitement with dense âwheelâ twins of superb sharpness and luster, establishing a modern benchmark. -> 20äžçŽåŸåãã«ã¶ãã¹ã¿ã³ã®Dzhezkazgané±åºã¯ãåè¶ããéããšå æ²¢ãæã€å¯éããâè»èŒªç¶âåæ¶ã«ãã£ãŠè奮ãåçãããçŸä»£ã®åºæºã確ç«ããŸããã
Butte, Montana produced distinctive lamellar and curved forms popular with locality collectors, and Tsumeb, Namibia yielded elegant matrix vugs with twinned plates on dolomite. -> ã¢ã³ã¿ãå·ãã¥ãŒãã¯ãå±å°çã³ã¬ã¯ã¿ãŒã«äººæ°ã®ããç¹åŸŽçãªèçç¶ããã³æ¹Ÿæ²åœ¢ãçã¿åºãããã ãšãïŒãããã¢ïŒã¯ãããã€ãäžã«åæ¶æ¿ãæã€äžåãªãããªãã¯ã¹ã®ç©ºæŽãç£åºããŸããã
Because truly fine crystals are uncommon and many older pieces sit in institutional or long-held private collections, the best examples command strong prices, with size, sharpness, contrast, and minimal alteration driving value. -> å®éã«æ¥µããŠè¯è³ªãªçµæ¶ã¯çšã§ãå€ãã®å€ãæšæ¬ã¯æ©é¢ã³ã¬ã¯ã·ã§ã³ãé·å¹Žä¿ç®¡ãããç§çã³ã¬ã¯ã·ã§ã³ã«åèµãããŠãããããæé«äŸã¯é«å€ãã€ããããšãå€ãããµã€ãºãã·ã£ãŒããã¹ãã³ã³ãã©ã¹ãããããŠæå°éã®æ¹å€ã䟡å€ãå·Šå³ããŸãã
Below are renowned sources known to have produced top-quality chalcocite specimens. Each locality link includes a map and image gallery. -> 以äžã¯é«å質ã®ãã£ã«ã³ãµã€ãæšæ¬ãçç£ãããšãããèåãªç£å°ã§ããåç£å°ã®ãªã³ã¯ã«ã¯å°å³ãšç»åã®ã£ã©ãªãŒãå«ãŸããŠããŸãã
Arguably the modern âtypeâ for showy chalcocite, Dzhezkazgan produced superb cyclic twins in the 1970sâ1990s. -> çŸä»£ã®ã·ã§ãŒåããã£ã«ã³ãµã€ãã®âåâãšããŠãããããDzhezkazganã¯1970幎代ãã1990幎代ã«ãããŠåè¶ãã埪ç°åæ¶ãçã¿åºããŸããã
Crystals are thick, pseudohexagonal plates and stacked rosettes with finely striated faces and a lustrous, dark steel-gray sheen. -> çµæ¶ã¯åããåœå è§åœ¢ã®æ¿ç¶ããã³ç©å±€ããŒãŒããã§ã衚é¢ã«ã¯çްããªçãå ¥ããå æ²¢ã®ããæãéŒéç°è²ã®å æ²¢ãæã¡ãŸãã
Many are freestanding clusters; matrix examples often feature pale carbonates for strong contrast. -> å€ãã¯èªç«ããã¯ã©ã¹ã¿ãŒã§ããããããªãã¯ã¹ã®äŸã«ã¯å¯Ÿæ¯ã匷ãããæ·¡è²ã®çé žå¡©é±ç©ããã°ãã°èŠãããŸãã
Choice pieces combine symmetry, sharp edges, and undisturbed terminationsâattributes that have made Dzhezkazgan chalcocite the reference standard for many collectors. -> éžããããã®æšæ¬ã¯å¯Ÿç§°æ§ãéããšããžããããŠæªæ¬ æã®çµç«¯ãçµã¿åãããŠãããDzhezkazganã®ãã£ã«ã³ãµã€ããå€ãã®ã³ã¬ã¯ã¿ãŒã®åç §æšæºã«ããŠããŸãã
Butte is famous for complex sulfide assemblages, and its chalcocite is distinctive: lamellar, sometimes curved or ârolled,â and often showing overgrowths or alteration rims to digenite or covellite that lend blue and purple tints. -> Butteã¯è€éãªç¡«åç©ã®ã¢ã»ã³ããªã§æåã§ããããã®ãã£ã«ã³ãµã€ãã¯ç¹åŸŽçã§ãïŒèçç¶ã§ãæã«ã¯æ¹Ÿæ²ãããâå·»ãããâ圢ç¶ããšãããã°ãã°ãã€ãžãã€ãïŒdigeniteïŒãŸãã¯ã³ãã©ã€ãïŒcovelliteïŒãžã®éæé·ã倿çžã瀺ããéè²ã玫è²ã®è²èª¿ã垯ã³ãŸãã
Well-composed clusters occur with quartz and calcite, and pseudomorphs or replacements among the copper sulfides add scientific interest. -> ç³è±ãšæ¹è§£ç³ãšã®çµã¿åããã§è¯å¥œã«æ§æãããã¯ã©ã¹ã¿ãŒãèŠãããé ç¡«åç©éã®æºåœ¢äœïŒpseudo morphsïŒã眮æãç§åŠçé¢å¿ãé«ããŸãã
Aesthetic Butte specimens can be excellent value and are historically significant to American mining. -> è¶£å³çãªButteæšæ¬ã¯éåžžã«äŸ¡å€ãé«ããã¢ã¡ãªã«ã®æ¡æå²ã«ãšã£ãŠæŽå²çã«ãéèŠã§ãã
In the midâlate 1800s, Bristol yielded some of the earliest truly fine chalcocite crystalsâsharp, tabular pseudohexagonal plates and rosettes, often on quartz or dolomite. -> 19äžçŽäžé ããåŸåã«ãããŠãããªã¹ãã«ã¯æãåæã®æ¬åœã«çŸãããã£ã«ã³ãµã€ãçµæ¶ãç£åºããŸããââéããæ¿ç¶ã®åœå è§åœ¢ã®æ¿ãšããŒãŒããã§ããã°ãã°ç³è±ããããã€ãäžã«ãããŸããã
Many classic East Coast collections feature âBristol chalcocite,â and well-documented pieces remain highly coveted today. -> å€ãã®ã¯ã©ã·ãã¯ãªæ±æµ·å²žã³ã¬ã¯ã·ã§ã³ã«ã¯âBristol chalcociteâãå«ãŸããããææžåãããæšæ¬ã¯çŸåšã§ãéåžžã«æ±ããããŠããŸãã
Although typically smaller than Dzhezkazgan giants, Bristol crystals exemplify textbook form and carry premium historical cachet. -> Dzhezkazganã®å·šæ¶ããã¯å°ããããšãå€ããã®ã®ãããªã¹ãã«ã®çµæ¶ã¯æç§æžçãªåœ¢ãäœçŸãããã¬ãã¢ã ãªæŽå²çè©äŸ¡ãæã£ãŠããŸãã
From the world-famous Tsumeb, chalcocite occurs as sharp twinned plates and rosettes in carbonate vugs. -> äžççã«æåãªãã ãšãé±å±±ã§ã¯ããã£ã«ã³ãµã€ãã¯çé žå¡©ã®ç©ºæŽå ã§éãåæ¶æ¿ãšããŒãŒãããšããŠçŸããŸãã
The best examples balance elegant form and high luster against light dolomite matrix, often accompanied by other copper species. -> æé«ã®æšæ¬ã¯ã軜ããããã€ãåºè³ªã«å¯ŸããŠåªé ãªåœ¢ç¶ãšé«ãå æ²¢ã®ãã©ã³ã¹ãåãããã°ãã°ä»ã®é ç¡«é»é±ç©ã䌎ããŸãã
As with many Tsumeb minerals, complex paragenesis and superb aesthetics increase desirability, and intact matrix specimens are prized. -> å€ãã®ãã ãšãé±ç©ãšåæ§ãè€éãªå ±çå²ãšåªããçŸèгãé åãé«ããæ¬ æã®ãªããããªãã¯ã¹æšæ¬ãé«ãè©äŸ¡ãããŸãã
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